1964
DOI: 10.1007/bf01116295
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Synthesis and physical identification of the isotope with mass number 260 of element 104

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Cited by 24 publications
(7 citation statements)
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“…The three experimental points given for element 104 represent (r n /T/) av values estimated from the experimental cross section 18 for the production of a 0.3-sec SF emitter in the reaction between 242 Pu and 22 Ne, assuming a 3n y 4w, and Sn reaction, respectively. Comparison with the extrapolated T n /T f values using both Eqs.…”
Section: Empirical Formula For T N /Tfmentioning
confidence: 99%
“…The three experimental points given for element 104 represent (r n /T/) av values estimated from the experimental cross section 18 for the production of a 0.3-sec SF emitter in the reaction between 242 Pu and 22 Ne, assuming a 3n y 4w, and Sn reaction, respectively. Comparison with the extrapolated T n /T f values using both Eqs.…”
Section: Empirical Formula For T N /Tfmentioning
confidence: 99%
“…Zvara et al [21,22] at the Joint Institute of Nuclear Research in Dubna developed an extremely fast on-line isothermal chromatographic method to study the volatility of Rf-chlorides on various column surfaces (stainless steel, teflon, glass). These experiments were designed to chemically identify an isotope of Rf decaying by spontaneous fission (SF) with a half-life of 0.3 s that was previously reported by a team of physicists at the same laboratory [23], and thus confirm the discovery of element 104. The existence of an isotope of Rf decaying by SF with a half-life of 0.3 s could not be confirmed, however [24].…”
Section: Introductionmentioning
confidence: 93%
“…Element 104 (Rf) was discovered in 1964 at JINR when the irradiation of a 242 Pu target by 115-MeV 22 Ne ions produced the isotope 260 Rf (T ½ = 0.3 s) (Flerov et al 1964), whereas the element 105 (Db) was identified in 1971 at LBNL by reactions of highly energetic 18 O and 16 O beams with 249 Bk targets (Ghiorso et al 1971).…”
Section: Elements 104-118: the Discoveringmentioning
confidence: 99%